The Future of the Aral Sea and its Ecosystem:
Possible scenarios and outcomes
H.P. Nachtnebel, V. Dukhovny, A. Tuchin, A. Sorokin,
Y. Roschenko, U. Uhalin, P.D. Umarov, B. Tashmukhamedov, I.
Contributing scientists
• SIC ICWC: V. Dukhovny, A. Sorokin, Y. Roschenko, R.
Kadirova
• Center of Intergrated Water Systems Research: A. Tuchin, P.D.
Umarov, U. Uhalin, A. Beloglazov, E. Korshak, E. Temlyanceva
• Institute of Physiology and Biophysics & Institute of Zoology at the Academy of Sciences, UZ
Bek Tashmukhamedov, I. Mirabdullayev
• Institute for Water and Environmental Problems of the Russian Academy of Sciences: O. Vasilyev, V.I. Kvon, V. I. Kuzin, A. N.
Semchukov, V. V. Martyanov
• IWHW-BOKU: H.P. Nachtnebel, Prof.H. Holzmann
Structure of the presentation
• Objectives and introduction
• Identification of scenarios for the Aral Sea region
• Assessment of scenarios
• Summary and conclusions
Objectives and introduction
The objective is to identify development strategies in the catchment
- to improve socio-economic development and water use in the region
- to achieve ecological sustainability and
bioproductivity in the Aral Sea and the
surrounding area
The Aral Sea catchment
The two tributaries
• Syrdarya (Jaxartes)
– 3019 km
– 782 670 km2
• Amurdarya (Oxus)
– 2400 km
– 534 739 km2
The two tributaries
• Syrdarya (Jaxartes)
– 3019 km
– 782 670 km2
• Amudarya
– 2400 km
– 534 739 km2
• Danube
Water sources and sinks
Some figures about water consumption in Central Asia
• Water sources
– 43% of the annual discharge in the basin originates in Tajikistan
– 24% in Kyrgyzstan
– approximately 19% in Afghanistan.
• water usage
– upstream mountain states use about 17%
– downstream Kazakhstan, Uzbekistan, and Turkmenistan use
Physical structure of WM
Hydrology: Inflow pattern
Changes of the Aral
Sea
Bathymetry of the Aral Sea
• Sea level until 1960 was about 53 m a.s.l.
• Surface was 69,8 10
3km
2• maximum depth was 69 m
• water volume was about 1056 km
3• about 1100 islands totaling 2 235 km
2existed
54 53 52 51 50 49 48 47 46 45 44 43 42 41 40 39 38 37 36 35 34 33 32 31 30 29.75 29.5 29.25 29 28 27 26 2524 23 22 2120 19 18 17 16 15 14 13 12 11 10 9 8 7 6 5
Fig. 4.1. Sink of the Aral Sea
Eastern part Western part
Northern part
Quantitative changes in the system
• Year Sea level Surface Volume (m.a.s.l.) 10
3km
2km
3• 1960 53,40 69,79 1056,12
• 1984 42,75 44,92 487,66
• 1986 41,02 38,56 380,63
• 2000 33,50 22,93 139,53
Development of water utilisation
Species composition (total number) in the Aral Sea
Taxa 1971 1981 1989 1994 2000 2001
zooplankton 43 18 13 9 8 5
zoobenthos 82 51 14 7 5
Fish 20 30 17 5 3 2
Salinity (g/l) 12 18 30 37 60 65
Some figures about salinity
• Salinity of regular sea waters 3,5 % 35g/l
• Brakish waters < 1% <10g/l
• Caspian Sea 1,3 % 13g/l
• Mono lake (Nevada) 7,3 % 73g/l
• Dead Sea ~30% 300g/l
Fish fauna
• Fish fauna in Aral Sea was relatively poor (20 species)
• Caspian Sea had 130 species
• Between 1950-1960 the # rose up to 30 species (introduction)
• With increase of salinity other species were introduced
• 1990 only 5 species were found
• 2001 only 2 species were found (atherine and
flounder)
Fauna
• Atherina Flounder
• Artemia
(from Wikipedia)
Main problems
• intensive cotton monoculture
• extreme environmental degradation
• Intensive pesticide use and salinization
• industrial pollution
• Irrigation lead to a decrease of surface and groundwater
• high rates of disease (cancer) and infant mortality.
Summary of changes
• Due to a dramatic drop in the influx of water into the Aral Sea, its area has been reduced to 25 %, the volume is now about 10%, the level dropped by 23 m
Summary of changes
• Due to a dramatic drop in the influx of water into the Aral Sea, its area has been reduced to 25 %, the volume is now about 10%, the level dropped by 23 m
• The Aral Sea has split into two water bodies, the Small Aral
(North) and the Large Aral (South). As a result, the water salinity in the Large Aral has grown by a factor of 7 reaching over 80 ppt in the Western basin and 100 ppt in the Eastern basin.
Summary of changes
• Due to a dramatic drop in the influx of water into the Aral Sea, its area has been reduced to 25 %, the volume is now about 10%, the level dropped by 23 m
• The Aral Sea has split into two water bodies, the Small Aral and the Large Aral. As a result, the water salinity in the Large Aral has grown by a factor of 7 reaching over 80 ppt in the Western basin and 100 ppt in the eastern basin.
• The Large Aral has turned into a polyhaline lake. As a result, this has brought about cardinal changes in the composition of
Summary of changes
• Due to a dramatic drop in the influx of water into the Aral Sea, its area has been reduced to 25 %, the volume is now about 10%, the level dropped by 23 m
• The Aral Sea has split into two water bodies, the Small Aral and the Large Aral. As a result, the water salinity in the Large Aral has grown by a factor of 7 reaching over 80 ppt in the Western basin and 100 ppt in the eastern basin.
• The Large Aral has turned into a polyhaline lake. As a result, this has brought about cardinal changes in the composition of the Aral biota. Most of the species disappeared
• The bio-productivity has extremely decreased
A dry region ?
• Yes and no !
Water Scarcity
• Indicators: Water Scarcity
– less than 1 700 m³ per year per person is available, people experience water stress.
– Less than 1 000 m³ per capita is classified as chronic water scarcity and
– less than 500 m³ as absolute water scarcity
• Rural Water Livelihoods Index (RWLI by FAO in 2009) It includes
– services component (access to water and sanitation), – security component (crop and livestock water),
– environment component (clean and healthy water), – entitlement component (secure and equitable water).
Water Scarcity
UNDP's 2006 Human Development Report
– The scarcity at the heart of the global water crisis is rooted in power, poverty and equality, not in physical availability.
– In many countries scarcity is the product of public policies that have encouraged overuse of water through subsidies and underpricing.
– There is more than enough water in the world for domestic purposes, agriculture and industry.
– The problem is that some people-notably the poor-are systematically excluded from access
Water availability (global)
Water Scarcity
What was done, what could be done ?
• Measures to improve the conditions of the lake
– Institutional set up
– Improving water governance (transboundary management) – Engineering measures
– Water management (improving water use efficiency)
Dublin Principles of 1992
• Fresh water is a finite and vulnerable resource, essential to sustain life, development and the environment;
• Water development and management should be based on a participatory approach, involving users, planners and policymakers at all levels;
• Women play a central part in the provision,
management and safeguarding of water;
Water management structure in the Soviet period
• early 1980-: average efficiency of irrigation systems (ratio of water used productively at the fields to headworks withdrawals) was around 60% in the Aral Sea basin, the lowest of any region in the Soviet Union
• In January 1988, a state committee for the protection of nature was formed, elevated as the Ministry for Natural Resources and Environmental Protection in 1990.
• The Ministry had authority over all aspects of the environment and the use of natural resources.
• Shortly after, the Interstate Coordination Water Commission (ICWC) was formed by the newly independent states to provide a platform for regional planning
.
Transboundary Management
• In February 1992, agreement to coordinate policies on their transboundary waters. Subsequent agreements in the 1990s and in 2002 have updated water management institutions
• 1992: an agreement to coordinate efforts to "solve the Aral Sea crisis"
– carrying out joint research – exchanging information
– adhering to agreed-to regulations for water use and protection.
– Establishment of a Commission for Water Management to
long term "Concept" and a short-term
"Program" for the Aral Sea
• 1994: Concept is based on a strict policy of water conservation. Allocation of water for preservation of the Aral Sea was recognized as a legitimate water use for the first time.
• four major objectives:
– to stabilize the environment of the Aral Sea;
– to rehabilitate the disaster zone around the Sea;
– to improve the management of international waters of the basin; and
– to build the capacity of regional institutions to plan and implement these programs.
Funding
• These regional activities are supported and supplemented by a variety of governmental and non-governmental agencies,
including the European Union, the World Bank, UNEP, and UNDP.
• 1995: Nukus Declaration indicated the need for a "unified multi- sectoral approach and the development of cooperation amongst the states and with the international community"
• 2002: Creation of the Central Asian Cooperation Organization (CACO) with a broad mandate to promote cooperation among
Lessons learned
• National objectives dominate basin wide interests.
• Lack of trust and credibility among the countries can hinder the process of cooperation.
• Water and energy resources are unequally distributed
• An inefficient water use
• Although a interstate committee has been established none of the plans was implemented
• The Central Asian Economic Community, now the Central Asian Cooperation Organization, playes a key role in mediating
between the Aral Sea Basin states when there were difficulties within the International Fund for the Aral Sea.
Measures in the South
Aral Sea and Priaralia region
f(t)
RS f(t) f(t)
SA w
SA e
SA m f(t)
The priaralie region: Amudarya Delta
d
d
d
d d d
d
d
d d
d d
d
$
d d
%
KKS SA-1
MA-1 RA-1 DU-1
KS-1
KS-3 DP-1 PP-1 DP-2
ÊÑ-4 AP-3
AP-1 AP-4
AP-5 AP-2
52.0
58.0 53.0
52.5 52.5 46.0
48.0 43.5
45.0
47.0
7 m3/s
36 m3/s
43 m3/s
24 m3/s
34 m3/s 10 m3/s 20 m3/s 44 m3/s
35 m3/s
39 m3/s
74 m3/s 38 m3/s
40 m3/s
93 m3/s
66 m3/s
36 m3/s
16 m3/s 25 m3/s 70 m3/s
10 m3/s
23 m3/s 44 m3/s
250 m3/s
140 m3/s
52.5 m3/s
1841 m3/s 1225 m3/s
1328 m3/s
1964 m3/s 1348 m3/s
1451 m3/s 2091 m3/s
1475 m3/s 1578 m3/s
Urdabai
Glavm
ya
so
Kazakhdarya
M
ashan-Karazhar
Inzh ener
ozek
Collecto r Ustyurt
Akkai
Ilenkul
Dumalak
Mashan ko l
Djiltyrbas res.
Muynak res.
Sudochye
Mejdurechenskoye Rybachie
Akdarya
Kun grad-M
uinak
Amu-Darya
Qopt = 2458 m3/ c Qint = 1842 m3/ c Qbus = 1945 m3/ c Water discharge in Samanbay
gauging station
Rivers Canals Collectors
Dams d Outlets
Hidrounints
$
% Escape Design:
52.5 ...Water surface elevations
Legend Water flows in scenarios
Optimistic Intermedium Business of usual
Saline water Mixed waters Optimistic Intermedium Business of usual Optimistic
Intermedium Business of usual Fresh water
Aral Sea
Variant I I I .
Corrected calculation by "Aral Consult"
Schematic map of water flow allocation in the years of maximum water supply
Measures to preserve the Aral Sea
The Northern part
In order to secure the existence of the Northern Aral Sea, Kazakhstan constructed, with a loan and
expertise from the World Bank, the
13-km Kok-Aral dike, which was
completed in 2005 and prevented
Planned Measures
Eastern part:
To preserve the Eastern part
(small surface and large volume) a
diversion from the Amudarya was
planned in 2000
Observed Improvements
• In addition to the dam
– old infrastructure on the Syr Darya was rehabilitated, – irrigation systems were improved
– several new hydraulic structures were constructed to reduce water losses and increase the flow of the Syr Darya.
– The surface of the Northern Aral Sea grew by 18% and the water rose by 2 meters.
– the salinity of the water, which had driven the fish into the
Observed biological improvements
• Biomass (weight of all the fish in the northern sea) was estimated in 2011 to have risen from 3 500 tonnes, most of it a flounder introduced from the
Black Sea, to 18 000 tonnes, most of it native, edible species like carp, pike perch, catfish and pike.
• Commercial fishing now accounts for 4 500 tonnes
and a fish-processing plant has started operating in
Aralsk, exporting the most valuable fish to Russia
and other neighbouring countries.
Water Management:
• Business as usual
• National visions
• Optimistic scenario
• Scenarios from 2006-2025
Scenarios from 2006-2025
• Business as usual
• National visions
• Optimistic scenario
also considering climatic variability (dry and wet)
also considering different water distribution systems
in the Deltas
Business as Usual
It is assumed that:
• The region will develop as usual regarding transboundary water management, each country is tending to self-provision in food production.
• Integration processes in transboundary water resources management will be developed slowly.
• Regional integration in agricultural production progresses poorly.
• Major national efforts are aimed at maintaining current water management and paying little attention to water conservation.
Toktogul Reservoir
• Construction period: 1962 – 1975
• Water surface of the reservoir: 284,3 km²
• Storage capacity: 19.500 Mio. m³
• Installed capacity: 1200 MW
Changes in reservoir management
Toktogul Reservoir (Kirgistan)
Was planned for irrigation + hydropower
National Future Development Strategies
• The national development plans of Kazakhstan, Kyrgyzstan, Tadjikistan, Usbekistan, Turkmenistan are analysed
• Indicators are growth rates of population, economic
development, resources use (land, water, energy..)
and social indicators (health, expected life time…)
Optimistic scenario (close co-operation)
Regional integrated development is supported by all the states:
• mutual beneficial use of transboundary water resources on the basis of water conservation and common environmental
approaches
• mutual beneficial agricultural development with focus on regional specialization in agricultural production
• Efficient water and resources use
• economic growth, mainly through industrial and services development
Analysis of the consequences
• Modelling and simulation tools hydrological model
water balance model
water management models agricultural models
economic model
ecological model (salinity, variability, depth)
• Impacts on the water bodies of Aral Sea
• Impacts on the Delta areas
• Impacts on the Priaralie region
An intensively managed catchment
Flow paths and consumers in the Amudarya catchment
Structure of the socio-economic model
Calibration of the
models
Simulation results
Salinity in the Eastern lake
54 53 52 51 50 49 48 47 46 45 44 43 42 41 40 39 38 37 36 35 34 33 32 31 30 29.75 29.5 29.25 29 28 27 26 25 24 23 22 21 20 19 18 17 16 15 14 13 12 11 10 9 8 7 6 5 4 3 2 1 0 -1 -2 -3 -4 -5 -6 -7 -8 -9 -10 -11 -12 -13 -14 -15 -16
Fig. 4.1. Sink of the Aral Sea
Eastern pa
Simulation results
Salinity in the Western lake
Seawater salinity
60,00 65,00 70,00 75,00 80,00 85,00 90,00 95,00 100,00
g/l
54 53 52 51 50 49 48 47 46 45 44 43 42 41 40 39 38 37 36 35 34 33 32 31 30 29.75 29.5 29.25 29 28 27 26 25 24 23 22 21 20 19 18 17 16 15 14 13 12 11 10 9 8 7 6 5 4 3 2 1 0 -1 -2 -3 -4 -5 -6 -7 -8 -9 -10 -11 -12 -13 -14 -15 -16
Fig. 4.1. Sink of the Aral Sea
Western part
Diversion of the input
Amudarya inflow goes to the Western lake
54 53 52 51 50 49 48 47 46 45 44 43 42 41 40 39 38 37 36 35 34 33 32 31 30 29.75 29.5 29.25 29 28 27 26 25 24 23 22 21 20 19 18 17 16 15 14 13 12 11 10 9 8 7 6 5 4 3 2 1 0 -1 -2 -3 -4 -5 -6 -7 -8 -9 -10 -11 -12 -13 -14 -15 -16
Fig. 4.1. Sink of the Aral Sea
Western part
Impacts on biology
Halotolerance of aquatic animals
Analysis of scenarios
• In all scenarios the Large Sea will separate into a Western and an Eastern lake
• The Eastern lake is very shallow, dries out from time to time and will have an extremely high salt
concentration
• The Western lake is deep, has a large volume and a small surface
• The salt concentration in the Western Sea will be
Analysis of scenarios
• The recent inflow from Amudarya feeds the Eastern part
• The runoff should be diverted to the Western part
• A compensation discharge should remain for the Amudarya Delta and the Priaralia shallow water bodies
• The biology and bioproductivity might be maintained in the Eastern part (??)
• Some autochthonous fish species may survive in
water bodies of the Priaralie region, if properly
managed
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
• Problems are due to water scarcity, inefficient water use and a lack of transboundary water management
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
• Problems are due to water scarcity, inefficient water use and a lack of transboundary water management
• Based on complex models three scenarios were analysed
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
• Problems are due to water scarcity, inefficient water use and a lack of transboundary water management
• Based on complex models three scenarios were analysed
• None is able to restore the Aral Sea
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
• Problems are due to water scarcity, inefficient water use and a lack of transboundary water management
• Based on complex models three scenarios were analysed
• None is able to restore the Aral Sea
• The major part of the lake is going to dry out soon
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
• Problems are due to water scarcity, inefficient water use and a lack of transboundary water management
• Based on complex models three scenarios were analysed
• None is able to restore the Aral Sea
• The major part of the lake is going to dry out soon
• The small Western part might be maintained
Summary and conclusions
• The historic development of the Aral Sea region was described for the last 50 years
• Problems are due to water scarcity, inefficient water use and a lack of transboundary water management
• Based on complex models three scenarios were analysed
• None is able to restore the Aral Sea
• The major part of the lake is going to dry out soon
• The small Western part might be maintained
• Parts of the biota may be preserved in the Delta regions
• In the long term the Western part might provide sufficiently low